Culture and Phylogenetic Characterization of Trichomitus trypanoides Duboscq & Grassè 1924, n. comb.: a Trichomonad Flagellate Isolated from the Hindgut of the Termite Reticulitermes santonensis Feytaud

ABSTRACT. A trichomonad flagellate strain R1 was isolated from the hindgut contents of the termite Reticulitermes santonensis Feytaud. The flagellate was cultivated at 28° C in anaerobic medium containing yeast extract, minerals and vitamins. The isolate fed on living bacteria. It showed the typical morphological and ultrastructural features of the trichomonads. closely resembling Trichomitus trypanoides. In order to determine its phylogenetic position the small subunit ribosomal DNA (SSU rDNA) of the flagellate was amplified in vitro using the polymerase chain reaction (PCR), cloned in a plasmid vector and sequenced. Comparison of the obtained sequence with so far available SSU rRNA/rDNA sequences showed strongest similarity (89%) to the sequence of Tritrichomonas foetus. The phylogenetic analysis with parsimony and distance matrix methods placed Trichomitus trypanoides strain R1 near by the root of the phylogenetically so far analyzed eukaryotic organisms. This confirms that termites harbour hindgut symbionts, which originate from very early evolved eukaryotes.     

Oceanic Anoxic Event at the Cenomanian–Turonian boundary interval (OAE-2): ichnological approach from the Betic Cordillera, southern Spain

Ichnological analysis of dark sediments of the Oceanic Anoxic Event at the Cenomanian–Turonian boundary interval (OAE-2) from the Betic Cordillera, southern Spain, reveals the presence of ichnofabrics containing trace fossils Chondrites isp., Palaeophycus heberti , Planolites isp., Thalassinoides isp., Trichichnus linearis , Zoophycos isp., and other bioturbational structures. Analysis of the ichnofabrics and trace fossil diversity allowed the reconstruction of relative oxygenation. Before the OAE-2, oxygenation of sediments was generally good, but it was punctuated by short anoxic events. During the OAE-2i, several longer anoxic intervals were interrupted by shorter dysaerobic and oxic periods. After the OAE-2, oxygenation improved and almost all trace fossils known before OAE-2 reappeared, although oxygenation dropped a few times to anoxia. Generally, the short oxygenation changes reveal a periodicity, which may suggest a Milankovitch control.     

Micro‐particle‐induced X‐ray emission mapping of elemental distribution in roots of a Mediterranean‐type sclerophyll,Agathosma betulina (Berg.) Pillans,colonized by Cryptococcus laurentii

The role of rhizosphere yeasts as plant nutrient‐scavenging microsymbionts in resource‐limited Mediterranean‐type heathlands is unknown. This study, therefore, focused on quantitative elemental distribution within the roots of a medicinal sclerophyll, Agathosma betulina (Berg.) Pillans, grown under nutrient‐poor conditions, and colonized by Cryptococcus laurentii. Micro‐particle‐induced X‐ray emission (PIXE) was used to assess quantitative elemental distribution within the roots of A. betulina inoculated with viable C. laurentii, as well as within roots of control plants that received autoclaved yeast. To aid in the interpretation of heterogeneous elemental distribution patterns, apoplastic barriers (Casparian bands) in root tissues were located using fluorescence microscopy. In addition, root cross‐sections were examined for endophytic C. laurentii using light and transmission electron microscopy (TEM). The average concentrations of P, Fe and Mn were significantly (P < 0.05) higher in roots of yeast‐inoculated plants, compared to control plants. Casparian bands were observed in the exodermal cells of both treatments, and the presence of these bands was correlated with elemental enrichment in the epi/exodermal‐outer cortical tissues. Light and TEM micrographs revealed that the yeast was not a root endophyte. This is the first report describing the role of a soil yeast as a plant nutrient‐scavenging microsymbiont.     

Four New Recent Genera of Foraminiferida

SYNOPSIS. Four new genera of Foraminiferida are described. Phlegeria , type species P. hyalina sp. nov. and Tomaculoides , type species T. lucidum sp. nov. belong to the family Glandulinidae, and both were obtained from the Gulf of Mexico. Francesita , type species Virgulina ? advena Cusbman is found in the North Atlantic and the Gulf of Mexico, and belongs to the Caucasinidae. Montfortella , type species M. bramlettei sp. nov. occurs in Pleistocene strata and is living on the coast of California, and belongs to the Cibicididae.     

N-methyl-N′-nitro-N-nitrosoguanidine and UV induced mutants of the dinoflagellate Crypthecodinium cohnii*

SYNOPSIS. Mutant strains were chemically induced by treatment with N-methyl-N′-nitro-N-nitrosoguanidine (NTG) and UV irradiation. UV and NTG mutation rates were obtained that were both consistent with the organism being haploid. Three types of mutants were produced: (a) strains deficient in both β- and γ-carotene, the only carotenoids found in the wild type; phenotypes include albinos (translucent, dull white, “snow white”) and cream-colored on agar as compared to the yellow-orange color of wild type colonies; (b) strains requiring adenine, guanine or cytosine in addition to the minimal medium for growth; (c) mutants that grow at a rate less than 40% of the wild type in minimal medium.